Results 71 to 80 of about 959 (180)
Abstract Marine cold‐air outbreak (MCAO) clouds begin as shallow cloud streets near the ice edge and evolve into broken open‐cell convection downstream. Their rapid transitions in cloud structure and microphysics are closely linked to vertical motions, but this interplay has not previously been observed from space. The EarthCARE satellite, carrying the
Jiseob Kim +3 more
wiley +1 more source
Large-eddy simulation (LES) is often used as a benchmark simulation in climate science and is suggested as a fundamental tool to examine, e.g., marine cloud brightening.
Matthias Schwarz +4 more
doaj +1 more source
The remarkable inefficiency of stratocumulus
Abstract. Marine stratocumulus clouds play a central role in Earth’s climate system by reflecting incoming solar radiation and exerting a strong cooling effect. Their organization into open and closed mesoscale cellular morphologies can be thought of as an example of bistable dynamics driven by aerosol–cloud interactions and mesoscale processes.
Benjamin Hernandez +4 more
openaire +2 more sources
Entrainment in stratocumulus‐topped mixed layers
AbstractMixed‐layer theory is used to synthesize and evaluate recently proposed entrainment parametrizations (rules) for the stratocumulus‐topped boundary layer. The results illustrate that recently proposed entrainment rules exhibit marked differences.
openaire +2 more sources
Characterization of HRRR-simulated rotor layer wind speeds and clouds along the coast of California [PDF]
Stratocumulus clouds, with their low cloud base and top, affect the atmospheric boundary layer wind and turbulence profile, thereby modulating wind energy resources.
J. Lee +5 more
doaj +1 more source
Marine stratocumulus convection
July 1977. ; Includes bibliographical references (pages 137-140). ; Sponsored by the GARP Section of the Office of Climate Dynamics, National Science Foundation ATM 76-09370.
Shubert, Wayne H., author +4 more
openaire +1 more source
How subtropical marine boundary layer (MBL) clouds respond to warming is investigated using large‐eddy simulations (LES) of a wide range of warmer climates, with CO2 concentrations elevated by factors 2–16. In LES coupled to a slab ocean with interactive
Zhihong Tan +3 more
doaj +1 more source
A new semi‐empirical turbulence parameterization is presented. Key features of the scheme include representation of turbulent diffusivities in terms of the turbulent kinetic energy that is determined by solving a quasi‐equilibrium form of the equation ...
Y. He, N. A. McFarlane, A. H. Monahan
doaj +1 more source
Slow Manifolds and Multiple Equilibria in Stratocumulus-Capped Boundary Layers
In marine stratocumulus-capped boundary layers under strong inversions, the timescale for thermodynamic adjustment is roughly a day, much shorter than the multiday timescale for inversion height adjustment. Slow-manifold analysis is introduced to exploit
Junya Uchida +2 more
doaj +1 more source
Stratocumulus clouds are cloud systems composed of stratiform clouds with embedded convective clouds, possessing strong catalytic potential and serving as key target cloud systems for weather modification operations.
Zhuo Liu +4 more
doaj +1 more source

